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<br />Q00881 <br /> <br />I <br /> <br />5 <br /> <br />i <br />.-:" <br />" <br />, <br /> <br />(B) Diversion Data 1943-1946 (Continued) <br /> <br />Comparative monthly, seasonal and annual diversions are shown in the <br /> <br />following tables J (pases 7, 8 & 9) as averases for the periods 1908-1942; <br /> <br /> <br />1908-1942 exclusive of the six flood years 1909, 1914, 1915, 1921, 1923 and <br /> <br /> <br />1942; and 1925-1941 (called for convenience, the 35 years, the 29 othsr <br /> <br /> <br />years and the ;1.7 years respectively) . These ,are oomparedwith ,the, 1943-1946 <br /> <br />period. Seasonal and annual averases are further sUllllllarized for the various <br /> <br />periods in summary Table J on pase 6 following. This table includes also <br /> <br />SUllllllaries of diversion data for the six flood years and for the median year <br /> <br />1908-1942. <br /> <br />Differences in the quantities of water diverted during the 1943-1946 <br /> <br />'. . .' . <br />period as compared with diversions during the various other pe~i~d~';';'e at~ <br /> <br />tributable to several conditions among \fhich are the operation of the John <br /> <br />Martin Reservoir, the inclusion or exclusion of years of , excessive water <br /> <br />supply in the pre-Caddoa period, water supply availability, irrigation re- <br /> <br />quirements, diversion and storage capacities and related conditions. <br /> <br />AS noted at the top of pase 4, the streamflows of the 1943-1946 period <br /> <br />resembled those of the 29 other years (exclusive of the six years of major <br /> <br /> <br />floods) . Thus comparison of the four years after Caddoa "i th this 29 year <br /> <br />..t!..,. .. <br /> <br />-<.~.~:- <br /> <br />0- <br />~~ J.~-,~ <br />